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Topographic LIDAR Surveys Topographic LIDAR Surveys for GIS Analyses in Coastal for GIS Analyses in Coastal
ParksParks
Jeremy Bracone, John Brock, Amar Nayegandhi
2006 ESRI User Conference
August 10, 2006
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ESRI User Conference 2006
TopicsPrevious studies relating to park management.
Current study – Topographic ComplexityDescription of MethodsAccuracy and UsefulnessQuestions and Future Goals
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ESRI User Conference 2006
Previous Park Management Studies
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
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ESRI User Conference 2006
Previous Park Management Studies
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
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Dune Inventory and MonitoringDune Inventory and Monitoring
Features and Attributes Features and Attributes associated with each dune:associated with each dune:
Date of 1Date of 1stst RecognitionRecognitionUnique Dune ID Unique Dune ID DuneDune--Only DEMOnly DEMBase ElevationBase ElevationBasal PolygonBasal PolygonDune Area Centroid Dune Area Centroid Location Location Total Dune AreaTotal Dune AreaTotal Dune VolumeTotal Dune Volume
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Centroid UTM Centroid UTM Easting, Northing: Easting, Northing: 488,903,4,234,526488,903,4,234,526Area: 10,031 mArea: 10,031 m22
Volume above Volume above baseline: 5,757 mbaseline: 5,757 m33
Date: 1998Date: 1998--0404--0909
4
Dune Inventory Dune Inventory and Monitoring and Monitoring –– Baseline MappingBaseline Mapping
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Dune Inventory Dune Inventory and Monitoring and Monitoring –– Change DetectionChange Detection
May 11, 2001April 3, 1998
1998: Single dune, volume = 5757m3
2001: Fragmented into three dunesVolume: major dune = 4853 m3, All 3 Combined = 5362 m3
488905,4234546
488903,4234526
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ESRI User Conference 2006
Previous Park Management Studies
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
![Page 9: Topographic LIDAR Surveys for GIS Analyses in Coastal Parks › gis › odyssey › 2006 › Presentations › Thursday … · Topographic LIDAR Surveys for GIS Analyses in Coastal](https://reader033.fdocuments.us/reader033/viewer/2022042323/5f0dca1f7e708231d43c1888/html5/thumbnails/9.jpg)
ESRI User Conference 2006
Previous Park Management Studies
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
![Page 10: Topographic LIDAR Surveys for GIS Analyses in Coastal Parks › gis › odyssey › 2006 › Presentations › Thursday … · Topographic LIDAR Surveys for GIS Analyses in Coastal](https://reader033.fdocuments.us/reader033/viewer/2022042323/5f0dca1f7e708231d43c1888/html5/thumbnails/10.jpg)
ESRI User Conference 2006
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ESRI User Conference 2006
Previous Park Management Studies
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
![Page 12: Topographic LIDAR Surveys for GIS Analyses in Coastal Parks › gis › odyssey › 2006 › Presentations › Thursday … · Topographic LIDAR Surveys for GIS Analyses in Coastal](https://reader033.fdocuments.us/reader033/viewer/2022042323/5f0dca1f7e708231d43c1888/html5/thumbnails/12.jpg)
ESRI User Conference 2006
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
Develop methods for extracting geomorphologic features from data
Detect and quantify dune formation and migrationShoreline mapping and monitoringMap shoreward edge of vegetation
Previous Park Management Studies
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ESRI User Conference 2006
Shoreward Edge of Vegetation
20011999
Shoreward Edge of Vegetation
20011999
Landward Retreatof Vegetation
Landward Retreatof Vegetation
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ESRI User Conference 2006
Determining Topographic Complexity
Rugosity – Surface Roughness + Vertical Relief
Important factor for assessing the complexity of coral reef habitats.
Rugosity is significant factor in controlling species diversity and distribution
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ESRI User Conference 2006
Determining Topographic Complexity
Measured in field by divers draping a chain along a transect.
Length of Chain / Linear Distance = Rugosity
Grayscale Satellite ImageryLight intensity is analyzed to derive rugosity
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Creation of synoptic topographic complexity
(rugosity) maps based on airborne lidar surveys
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ProblemsCurrent Rugosity algorithm heavily biased towards areas with high slope.
Makes distinguishing between a rough slope and a smooth slope impossible
Rugosity calculations for steep fringing reefs will primarily reflect slope.
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Surface ComplexitySurface Complexity (or roughness) differs from Rugosity
Examines the roughness of the surface after compensating for topographic relief
Unit change to percent:Percent more complex than a flat surface
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ESRI User Conference 2006
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Methods
Gridding Process
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Modeled with
10x VerticalExaggeration
% complexity
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ESRI User Conference 2006
Current Studies Utilizing Rugosity
Study of the development of the FL Keys.Hypothesis:●Rugosity increases southeastward towards older reef
structures due to reef decay●Can be used as an indicator for reef maturity
Utilizing Rugosity as an indicator of species diversity.
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ESRI User Conference 2006
Future Inquiries into New Algorithm
How do different surface complexity values relate to habitat?
Is there a relationship between surface complexity value and substrate?
Is a smaller kernel size more useful for surface and substrate relationships?
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AcknowledgementsNASA Wallops Flight FacilityWallops Island, VA
U.S. Geological SurveyCenter for Coastal and Watershed Studies, FL
National Park ServiceSoutheast / Caribbean NetworkNortheast NetworkGulf Islands Network
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ESRI User Conference 2006
Integrated Remote Sensing and Modeling Group Website:
http://coastal.er.usgs.gov/remote-sensing/